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L <- lipdR::readLipd("https://lipdverse.org/data/QsrMCFTlFOvTZfxNCKKi/1_0_10/TR04EVLI.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: Wood
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/6111
lipdVersion: 1.3
author: list(name = "Evans M. N.")
doi: 10.1016/j.gca.2004.01.006
latitude: 10
longitude: -85
elevation: 300
siteName: Liberia, Costa Rica
TSid: MAT72a4e2b7ed
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: MATafd8e59e6e
variableName: depth
units: cm
description: depth
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: TR04EVLI01
variableName: d18O
units: permil
description: cellulose
basis: The range of the observed 18O cyclicity, 3a€“5a€°, is approximately equal to the annual range of observed rainfall d18O values (IAEA/WMO, 2003) for stations from Honduras, Costa Rica and Panama.
direction: negative
scope: climate
variable: precipitation
variableDetail: Seasonal, annual
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_amount
scope: climate
scope: climate
basis: Sub-annual cyclic isotopic signatures of several permil represent the annual cycle of local rainfall and relative humidity. Additional data from a plantation tree of known age from ENSO-sensitive northwestern coastal Peru suggests that the 1997–8 ENSO warm phase event was recorded as an 8‰ anomaly in the δ18O of α-cellulose.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeUncertainty: 5
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
scope: isotope
scope: isotope
root
pub
pub1
pub2
geo
PaleoData columns
year (yr AD)
interpretation
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2
3
depth (cm)
interpretation
1
2
3
d18O (permil)
interpretation
1
2
3
4
5
6